Electromagnetic Imaging and Simulated Annealing

In contrast with acoustical imaging methods, for which the wave field is dominated by propagation effects, electromagnetic imaging of conductive media suffers from the diffusive behavior of the electromagnetic field. An important question to address when working toward the achievement of electromagnetic imaging concerns the possibility of resolving the diffusion damping. Exact inversion will be looking at the solvability of the integral equation relating a diffusive field to its dual wavefield. This equation is ill posed because its Laplace-like kernel makes the inverse problem of finding the dual wave field a notoriously difficult (both numerically and mathematically) one. Stochastic inversion is another alternative based on least squares fitting. In this inverse problem approach, extracting the wave field is still a relatively instable process, although the L2 misfit function for data without noise presents a global minimum. The simulated annealing overcomes this instability for parameterization of this problem designed as follows. The unknown wave field is expected to be a sequence of impulsive functions. The number of impulsive functions can be determined by using a statistical criterion, called AIC, which comes from the Prony technique. The simulated annealing is applied to the positions of the reflections, while the amplitudes, which are not taken as parameters, are obtained by linear fitting. The simulated annealing method proves to be efficient even in the presence of noise. Furthermore, this nonlinear numerical inversion furnishes statistical quantities which allows an estimation of the resolution. Simple synthetic examples illustrate the performance of the inversion, while a synthetic finite element example shows the final pseudo-seismic section to be processed by standard seismic migration techniques.

[1]  Thomas Kailath,et al.  Detection of signals by information theoretic criteria , 1985, IEEE Trans. Acoust. Speech Signal Process..

[2]  Bruce E. Hajek,et al.  Cooling Schedules for Optimal Annealing , 1988, Math. Oper. Res..

[3]  Huang,et al.  AN EFFICIENT GENERAL COOLING SCHEDULE FOR SIMULATED ANNEALING , 1986 .

[4]  D. Oldenburg,et al.  Inversion of electromagnetic data: An overview of new techniques , 1990 .

[5]  C. D. Gelatt,et al.  Optimization by Simulated Annealing , 1983, Science.

[6]  de Raedt H,et al.  Calculation of the director configuration of nematic liquid crystals by the simulated-anneal method. , 1988, Physical review. A, General physics.

[7]  M. M. Lavrentʹev,et al.  Ill-Posed Problems of Mathematical Physics and Analysis , 1986 .

[8]  M. A. Frenkel,et al.  The solution of the inverse problems on the basis of the analitical continuation of the transient electromagnetic field in the reverse time. , 1983 .

[9]  P. Weidelt The inverse problem of geomagnetic induction , 1973 .

[10]  Rammile Ettelaie,et al.  Zero-temperature scaling and simulated annealing , 1987 .

[11]  Alan C. Tripp,et al.  Two-dimensional resistivity inversion , 1984 .

[12]  J. Wang,et al.  Subsurface imaging using magnetotelluric data , 1988 .

[13]  Daniel H. Rothman,et al.  Nonlinear inversion, statistical mechanics, and residual statics estimation , 1985 .

[14]  Monte Carlo Analysis of Geophysical Inverse Problems , 1991 .

[15]  Wafik B. Beydoun,et al.  Reference velocity model estimation from prestack waveforms: Coherency optimization by simulated annealing , 1989 .

[16]  Emile H. L. Aarts,et al.  Simulated Annealing: Theory and Applications , 1987, Mathematics and Its Applications.

[17]  S.M. Kay,et al.  Spectrum analysis—A modern perspective , 1981, Proceedings of the IEEE.

[18]  I ScottKirkpatrick Optimization by Simulated Annealing: Quantitative Studies , 1984 .

[19]  J. Hadamard,et al.  Le problème de Cauchy et les équations aux dérivées partielles linéaires hyperboliques : leçons professées à l'Université Yale , 1932 .

[20]  C. Barnett Simple inversion of time-domain electromagnetic data , 1984 .

[21]  Gerald W. Hohmann,et al.  Integral equation solution for the transient electromagnetic response of a three-dimensional body in a conductive half-space , 1985 .

[22]  V. Cerný Thermodynamical approach to the traveling salesman problem: An efficient simulation algorithm , 1985 .

[23]  G. Kunetz,et al.  PROCESSING AND INTERPRETATION OF MAGNETOTELLURIC SOUNDINGS , 1972 .

[24]  Karl Heinz Hoffmann,et al.  On lumped models for thermodynamic properties of simulated annealing problems , 1988 .

[25]  Gerald W. Hohmann,et al.  Electromagnetic modeling of three-dimensional bodies in layered earths using integral equations , 1983 .

[26]  Raj Mittra,et al.  Problems and solutions associated with Prony's method for processing transient data , 1978 .

[27]  Michael Creutz,et al.  Monte Carlo Study of Quantized SU(2) Gauge Theory , 1980 .

[28]  P. Weidelt,et al.  Inversion of two-dimensional conductivity structures , 1975 .

[29]  George A. McMechan,et al.  Phase‐field imaging: The electromagnetic equivalent of seismic migration , 1987 .

[30]  Nulton,et al.  Statistical mechanics of combinatorial optimization. , 1988, Physical review. A, General physics.

[31]  Ki Ha Lee,et al.  A new approach to modeling the electromagnetic response of conductive media , 1989 .

[32]  Philip E. Wannamaker,et al.  PW2D finite element program for solution of magnetotelluric responses of two-dimensional earth resistivity structure. User documentation , 1985 .

[33]  Daniel H. Rothman,et al.  Automatic estimation of large residual statics corrections , 1986 .

[34]  Gerald W. Hohmann,et al.  Diffusion of electromagnetic fields into a two-dimensional earth; a finite-difference approach , 1984 .

[35]  L N Frazer,et al.  Rapid Determination of the Critical Temperature in Simulated Annealing Inversion , 1990, Science.

[36]  P. Tarits Contribution des sondages electromagnetiques profonds a l'etude du manteau superieur terrestre , 1989 .

[37]  W. Huggins,et al.  Best least-squares representation of signals by exponentials , 1968 .